An abrupt increase in rainfall during the monsoon season in Asia could have a strong impact on many activities of two thirds of the world's population, including agriculture, commerce, forestry, and hydropower. Over Southeast Asia, rapid precipitation enhancement mainly occurs during commencement of the Asian summer southwest monsoon, which signifies a transition from the dry to the rainy season (Lau & Yang, 1997;Nguyen-Le et al., 2015;Zhang et al., 2002). Therefore, research in past decades has increasingly focused on the summer monsoon onset date (SMOD) or summer rainy season onset date (RSOD). For example, Zhang et al. (2002) used the observed daily rainfall over the central Indochina Peninsula (ICP) to determine the mean SMOD as being May 9, with a standard deviation of 12 days. Applying the empirical orthogonal function analysis on daily mean precipitation, Nguyen-Le et al. (2015) demonstrated that the mean summer RSOD over the eastern ICP is May 6, with a standard deviation of 13 days. However, the immediate increase in rainfall over the eastern ICP is observed in early autumn when the summer monsoon withdraws (